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    Effects of Pressure on Collision, Coalescence, and Breakup of Raindrops. Part I: Experiments at 50 kPa

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 008::page 2190
    Author:
    List, Roland
    ,
    Fung, C.
    ,
    Nissen, R.
    DOI: 10.1175/2009JAS2863.1
    Publisher: American Meteorological Society
    Abstract: Previous breakup experiments have been carried out at laboratory pressures (?100 kPa). However, raindrop interactions mainly take place higher up in the atmosphere, even in the supercooled part of a cloud where drops can be initiated by shedding from hailstones. Thus, 50 kPa, corresponding to a height of ?5.5 km in the atmosphere at a temperature of ??20°C, was selected to bracket the region of interest for rain. Six drop pairs were studied at 50 kPa and laboratory temperature (?20°C), one of them with reduced surface tension. The apparatus consists of drop-producing nozzles, acceleration systems, deflectors, a timing and selection control, a pressure regulator, and a photographic unit, mostly set up in a low-pressure chamber. After acceleration to terminal speed, a smaller drop is blown into the path of the larger one while an electronic timing system selects suitable drop pairs that may collide, thereby triggering eight subsequent flashes with a frequency of up to 100 kHz. The results are displayed in terms of a normalized fragment probability per size bin, ready for parameterization in the Part II of this paper. Five drop pairs were studied in 772 individual events. Overall, 51% resulted in filament breakup, 22% in sheet breakup, 7% in disk breakup, and 20% ended in coalescence. No bag breakups were observed. When compared to the 100-kPa results, the fragment numbers increased at large collision kinetic energies (CKEs) by factors of between 2.64 and 4.37 with pressure decreasing from 100 to 50 kPa, and they remained unchanged at low CKE. Detailed diagrams and tables show the results for the different drop pairs and collision categories. Increasing the sensitivity of the optical measurements from 0.05 to 0.01 cm increased the number of recognized fragments by factors up to 4.4, but only for the two higher-CKE cases. The higher resolution did not increase the fragment numbers detected in the lower-CKE range.
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      Effects of Pressure on Collision, Coalescence, and Breakup of Raindrops. Part I: Experiments at 50 kPa

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4209946
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    contributor authorList, Roland
    contributor authorFung, C.
    contributor authorNissen, R.
    date accessioned2017-06-09T16:28:05Z
    date available2017-06-09T16:28:05Z
    date copyright2009/08/01
    date issued2009
    identifier issn0022-4928
    identifier otherams-68393.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4209946
    description abstractPrevious breakup experiments have been carried out at laboratory pressures (?100 kPa). However, raindrop interactions mainly take place higher up in the atmosphere, even in the supercooled part of a cloud where drops can be initiated by shedding from hailstones. Thus, 50 kPa, corresponding to a height of ?5.5 km in the atmosphere at a temperature of ??20°C, was selected to bracket the region of interest for rain. Six drop pairs were studied at 50 kPa and laboratory temperature (?20°C), one of them with reduced surface tension. The apparatus consists of drop-producing nozzles, acceleration systems, deflectors, a timing and selection control, a pressure regulator, and a photographic unit, mostly set up in a low-pressure chamber. After acceleration to terminal speed, a smaller drop is blown into the path of the larger one while an electronic timing system selects suitable drop pairs that may collide, thereby triggering eight subsequent flashes with a frequency of up to 100 kHz. The results are displayed in terms of a normalized fragment probability per size bin, ready for parameterization in the Part II of this paper. Five drop pairs were studied in 772 individual events. Overall, 51% resulted in filament breakup, 22% in sheet breakup, 7% in disk breakup, and 20% ended in coalescence. No bag breakups were observed. When compared to the 100-kPa results, the fragment numbers increased at large collision kinetic energies (CKEs) by factors of between 2.64 and 4.37 with pressure decreasing from 100 to 50 kPa, and they remained unchanged at low CKE. Detailed diagrams and tables show the results for the different drop pairs and collision categories. Increasing the sensitivity of the optical measurements from 0.05 to 0.01 cm increased the number of recognized fragments by factors up to 4.4, but only for the two higher-CKE cases. The higher resolution did not increase the fragment numbers detected in the lower-CKE range.
    publisherAmerican Meteorological Society
    titleEffects of Pressure on Collision, Coalescence, and Breakup of Raindrops. Part I: Experiments at 50 kPa
    typeJournal Paper
    journal volume66
    journal issue8
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/2009JAS2863.1
    journal fristpage2190
    journal lastpage2203
    treeJournal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 008
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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